Abstract

Abstract. Anaerobic decomposition of organic carbon (OC) in submerged rice paddies is coupled to the reduction of alternative soil electron acceptors, primarily Fe3+. During reductive dissolution of Fe3+ from pedogenic oxides, previously adsorbed native soil organic carbon (SOC) could be co-released into solution. Incorporation of crop residues could hence indirectly, i.e. through the stimulation of microbially mediated Fe3+ reduction, promote the loss of native SOC via enhanced dissolution and subsequent mineralisation to CO2 and CH4. Our aim was to estimate the relevance of such a positive feedback during the degradation of added OC, and to investigate the impact of irrigation management on this mechanism and on priming effects on native SOC decomposition in general. In a six-week pot experiment with rice plants, two Bangladeshi soils with contrasting SOC to oxalate-extractable Fe (SOC : Feox) ratios were kept under a regime of alternate wetting and drying (AWD) or continuous flooding (CF), and were either amended with maize shoots or not. The δ13C signatures of dissolved organic C and emitted CH4 and CO2 were used to infer the decomposition of added maize shoots (δ13C = −13.0 ‰) versus native SOC (δ13C = −25.4 ‰ and −22.7 ‰). Addition of maize residues stimulated the reduction of Fe as well as the dissolution of native SOC, and the latter to a larger extent under CF, especially for the soil with the highest SOC : Feox ratio. Estimated Fe-bound SOC contents denote that stimulated SOC co-release during Fe reduction could explain this positive priming effect on SOC dissolution after the addition of maize. However, priming effects on SOC mineralisation to CO2 and CH4 were lower than for SOC dissolution, and were even negative under AWD for one soil. Enhanced reductive dissolution of Fe-bound SOC upon exogenous OC addition therefore does not necessarily lead to stimulated SOC mineralisation. In addition, AWD irrigation was found to decrease the above-mentioned priming effects.

Highlights

  • Anaerobiosis in flooded paddy fields thoroughly affects soil chemical processes, as in the absence of oxygen, the decomposition of organic carbon (OC) requires alternative terminal electron acceptors like manganese (Mn4+), iron (Fe3+), sulphate, acetate or carbon dioxide (CO2)

  • Fe concentrations after 11 d after transplanting (DAT) dropped to lower levels in the case of AWD compared to continuous flooding (CF) (P < 0.001 for Balina and P = 0.04 for Sonatala)

  • Using a stable isotope approach, it was confirmed that the addition of high-quality OC like maize shoots stimulates Fe reduction and dissolution of native soil organic carbon (SOC)

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Summary

Introduction

Anaerobiosis in flooded paddy fields thoroughly affects soil chemical processes, as in the absence of oxygen, the decomposition of organic carbon (OC) requires alternative terminal electron acceptors like manganese (Mn4+), iron (Fe3+), sulphate, acetate or carbon dioxide (CO2). Anaerobic reduction of the latter two electron acceptors, which depends on the production of dissolved organic carbon (DOC) as an electron donor, leads to the production and emission of methane (CH4) (Kögel-Knabner et al, 2010; Ponnamperuma, 1972). This limited insight mainly stems from difficulties in discerning native SOC and exogenous OC mineralisation based

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